numerical prediction and correction of tidal forcing for kaohsiung second harbor using roms

Numerical Prediction and Correction of Tidal Forcing for Kaohsiung Second Harbor Using ROMS Institute of Ocean Engineering and Technology, National Kaohsiung Marine University, Taiwan, R.O.C. E-Mail address: [email protected] Ho-Shuenn Huang Particle trajectories (floater) on the water surface, a post-calculation. The configuration of constructing a numerical ocean model in monitoring and predicting ocean dynamics. The water height at sea surface and the corresponding velocity vectors. (The left pictures: high tide; the right pictures: low tide.) 2010 ROMS/TOMS User Workshop, Hawaii, U.S.A. April 05 ~ 08, 2010 This study attempts to investigate and then predict the ocean dynamics ne ighboring Kaohsiung Second Harbor in Taiwan by utilizing ROMS. Effects of t idal forcing and current are presently involved in numerical simulations whi le comparing with the measured sea level data from the NKMU buoy and/or othe r units. The terrain of the computational domain over the Kaohsiung Second Harbor is input according to the given geographic coordinates (longitude and latitu de) to form the bathymetry file. Then, SEAGRID or EASYGRID generate the gri ds which are nearly orthogonal. There are in total 139 (east, west) × 139 (south, north) × 20 (depth) grid resolutions. During the numerical simulati ons, a time step of 2 sec is selected for securing the stable CFL condition. Tidal forcing is specified on the southern boundary, in which case the fre e-surface Chapman condition and 2D momentum Flather condition are utilized. Open boundary conditions with 3D momentum radiation conditions are also impo sed. It was found that the proposed numerical models were able to fairly pr edict the sea level of the tidal forcing and current nearby Kaohsiung Second Harbor where there existed irregular changeovers of the diurnal and semi-diu rnal tides. Satellite Maps, Geographic Maps, Terrain Maps, Sea Maps. Grids Generation, ROMS Simulations, Output : Matlab (Figur es), Ocean Dynamic s. (At Fixed Location) Oceanic Parameters, e.g., History of Sea Level and Its Predicted Trend. (At Fixed Location) Comparing, Calibrating, and Predicting (Statistical Methods). Real- Time Data Input Central Weather Bureau (Taiwan) Radar Scanning Equipment (Mobile) NKMU Buoy (Fixed Location) Real- Time Data Display The author would like to thanks the supports of computer resources from NKMU and supports of funding from Bureau of Education, Taiwan (R.O.C.). A Comparison of the measured water height from CWB and NKMU buoy, and the predicted from ROMS.

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Numerical Prediction and Correction of Tidal Forcing for Kaohsiung Second Harbor Using ROMS

Institute of Ocean Engineering and Technology, National Kaohsiung Marine University, Taiwan, R.O.C.E-Mail address: [email protected]

Ho-Shuenn Huang

Particle trajectories (floater) on the water surface, a post-calculation.

The configuration of constructing a numerical ocean model in monitoring and predicting ocean dynamics.

The water height at sea surface and the corresponding velocity vectors.(The left pictures: high tide; the right pictures: low tide.)

2010 ROMS/TOMS User Workshop, Hawaii, U.S.A. April 05 ~ 08, 2010

This study attempts to investigate and then predict the ocean dynamics neighboring Kaohsiung Second Harbor in Taiwan by utilizing ROMS. Effects of tidal forcing and current are presently involved in numerical simulations while comparing with the measured sea level data from the NKMU buoy and/or other units.

The terrain of the computational domain over the Kaohsiung Second Harbor is input according to the given geographic coordinates (longitude and latitude) to form the bathymetry file. Then, SEAGRID or EASYGRID generate the grids which are nearly orthogonal. There are in total 139 (east, west) × 139 (south, north) × 20 (depth) grid resolutions. During the numerical simulations, a time step of 2 sec is selected for securing the stable CFL condition. Tidal forcing is specified on the southern boundary, in which case the free-surface Chapman condition and 2D momentum Flather condition are utilized. Open boundary conditions with 3D momentum radiation conditions are also imposed. It was found that the proposed numerical models were able to fairly predict the sea level of the tidal forcing and current nearby Kaohsiung Second Harbor where there existed irregular changeovers of the diurnal and semi-diurnal tides.

Satellite Maps, Geographic Maps, Terrain Maps,Sea Maps.

Grids Generation, ROMS Simulations,Output : Matlab (Figures), Ocean Dynamics.

(At Fixed Location)Oceanic Parameters, e.g., History of Sea Level and Its Predicted Trend.

(At Fixed Location)Comparing, Calibrating, and Predicting (Statistical Methods).

Real-TimeDataInput

Central Weather Bureau (Taiwan)

Radar Scanning Equipment (Mobile)

NKMU Buoy (Fixed Location)

Real-TimeData

Display

The author would like to thanks the supports of computer resources from NKMU and supports of funding from Bureau of Education, Taiwan (R.O.C.).

A Comparison of the measured water height from CWB and NKMU buoy, and the predicted from ROMS.